FN Archimer Export Format
PT J
TI Comment on "Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach" by Wenyue Xu and Leonid N. Germanovich - art. no. B02103
BT 
AF SULTAN, Nabil
AS 1:1;
FF 1:PDG-DOP-DCB-GM-LES;
C1 IFREMER, Dept Geosci Marines, F-29280 Plouzane, France.
C2 IFREMER, FRANCE
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
IF 2.953
TC 41
UR https://archimer.ifremer.fr/doc/2007/publication-2318.pdf
LA English
DT Article
DE ;pore pressure;hydrate;dissolution;Dissociation
AB While it is well accepted that gas hydrate dissociation at the base of the Gas Hydrate Stability Zone (GHSZ) can generate high excess pore pressure and leads to sediment deformation, the consequence in terms of pore pressure of the dissolution of the gas hydrate at the top of the Gas Hydrate Occurrence Zone (GHOZ) remains neglected. The purpose of this comment on Xu and Germanovich [2006] article is to demonstrate that gas hydrate dissolution in the GHSZ may generate excess pore pressure and to point out the risk related to hydrate dissolution at the top of the GHOZ.
PY 2007
PD FEB
SO Journal of Geophysical Research
SN 0148-0227
PU American Geophysical Union
VL 112
IS B2
UT 000244374300006
DI 10.1029/2006JB004527
ID 2318
ER

EF